The
Upper Rhine Plain,
Rhine Rift Valley or
Upper Rhine Graben (
German:
Oberrheinische Tiefebene,
Oberrheinisches Tiefland or
Oberrheingraben,
French:
Vallée du Rhin) is a major
rift, about 350 km long and on average 50 km wide, between the cities of
Frankfurt/
Wiesbaden in the north and
Basel in the south. Its southern section straddles the border between
France and
Germany. It forms part of the
European Cenozoic Rift System, which extends across central Europe. The Upper Rhine Graben formed during the
Oligocene as a response to the evolution of the
Alps to the south and remains active to the present day. Today, the Rhine Rift Valley forms a downfaulted trough through which the
River Rhine flows.